Rivers Flashcards

1
Q

What type of erosion happens more in the lower course?

A
  • lateral erosion
  • gradient is flatter so river meanders find the best route to sea
  • so more erosion on outer part of river
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2
Q

What is a meander?

A

a bend in the river’s channel

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3
Q

What are the main features of a meander?

A
  • thalweg
  • deposition on the inside bend
  • erosion on the outside bend
  • river beach/slip-off slope
  • river cliff
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4
Q

How are meanders formed?

A
  • river erodes laterally & migrates across valley floor over time, widening valley
  • when river reaches meander, most water goes to outer bend & erosion occurs here, since there is less friction as the water is deeper
  • abrasion & hydraulic action undercut outside of river bend forming a river cliff
  • sand & small pebbles are deposited creating a gentle slip off slope on the inside bend since water is shallower & there is more friction
  • this continues
  • over time, meander will become tighter forming a swans neck & possibly oxbow lake
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5
Q

How is an oxbow lake formed?

A
  • continued erosion on outer bend of meander where river flows fastest
  • deposition continues on inside bend, causing slip off slope to grow
  • so outside bends of meander move closer together as meander neck becomes narrower
  • swan’s neck meander as 2 meanders move closer together
  • during a period of high discharge (maybe a flood) river cuts through neck to shorten the source
  • fastest current now flows in centre of channel & deposition means original meander is blocked off leaving an oxbow lake
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6
Q

Describe the characteristics of a river’s drainage basin?

A
  • rivers begin upland & flow downstream, become wider until the enter the sea
  • source is where the river begins & where it ends is the mouth
  • other smaller rivers (tributaries) join the main river at the confluence
  • the area drained by a river is the drainage basin
  • the boundary of this is the water shed, often a ridge of high land
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7
Q

What is the hydrological cycle?

A
  1. evaporation
  2. transpiration
  3. condensation
  4. precipitation
  5. surface run-off
  6. infiltration
  7. percolation
  8. groundwater flow
  9. throughflow
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8
Q

What is precipitation?

A

any source of moisture reaching the ground, e.g. rain, snow, hail

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9
Q

What is transpiration?

A

water loss through pores in vegetation

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10
Q

What is throughflow?

A

water flowing through the soil layer parallel to the surface

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11
Q

What is groundwater?

A

water stored in the rock

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12
Q

What is soil moisture?

A

water held in the soil layer

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13
Q

What is surface storage?

A

water held on the ground surface e.g. puddles

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14
Q

What is percolation?

A

water seeping deeper below the surface

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15
Q

What is groundwater flow?

A

water flowing through the rock layer

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16
Q

What is evaporation?

A

water lost from the ground surface

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16
Q

What is surface run off?

A

water flowing on top of the ground

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16
Q

What is infiltration?

A

water sinking into soil/rock from the surface

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17
Q

What is interception?

A

water being prevented from reaching the surface by trees & grass

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18
Q

What is a floodplain?

A

flat area adjacent to the river channel, mainly in the lower part of the course

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19
Q

What are levees?

A

raised banks along the course of the river in the lower course, formed naturally but can be artificially increased in height

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20
Q

How are floodplains formed?

A
  • river widens by lateral erosion, taking away interlocking spurs present nearer the source & a flat, wide area is created
  • at times of high discharge, river has high amounts of energy, which transports large amounts of material
  • when river overflows it will spread out across the surrounding flat land
  • sudden increase in friction will reduce the water’s velocity & fine silt will be deposited
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21
Q

How are levees formed?

A
  • each time the river floods, another layer of silt is added, forming a flat floodplain
  • largest material will be deposited first, forming a natural embankment (a levee)
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22
Q

What are deltas?

A

found at mouth of river, where it meets the sea, usually triangular in shape with top of delta having flat surface

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23
Q

How are deltas formed?

A
  • sediment brought downstream, as velocity decreases deposition occurs
  • heaviest load deposited first
  • finer particles carried into deeper water & when dropped divides river into separate channels called distributaries
  • because there is no current the material grows to sea & the distributaries rejoin
  • deposition continues so it builds upwards & outwards, over time vegetation will colonise the area
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24
Q

How are interlocking spurs formed?

A
  • vertical erosion in upper course creates v-shaped valley, that is steep sided & narrow
  • as river erodes downwards, soil & loose rock on valley sides are moved downhill by slopewash/soil creep
  • material is then added to load of river
  • river has to wind around hills, called interlocking spurs
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25
Q

How are waterfalls formed?

A
  • layer of hard rock lays over a layer of soft rock, water begins to erode soft rock that is less resistant, creating a steep gradient
  • erosion of less resistant rock underneath, undercuts hard rock above, hydraulic action & abrasion create a plunge pool at foot of waterfall
  • ledge that overhangs plunge pool eventually collapses under it’s own weight, debris is then eroded by hydraulic action & attrition, material is then transported downstream
  • waterfall takes a position further back
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26
Q

What is a gorge?

A

very steep sided valley

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27
Q

How is a gorge formed?

A

as a waterfall continues to retreat upstream

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28
Q

What are potholes?

A

if a river bed is uneven, pebbles can become trapped & swirling currents cause the pebbles to rotate & erode circular holes in the river bed

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29
Q

What is the channel?

A

part of river valley occupied by water

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30
Q

What is hydraulic action?

A

when air is forced into cracks in river banks by flow of water, causing them to widen & break down

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31
Q

What is attrition?

A

load carried by the river collides causing it to break into smaller, more rounded pieces

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32
Q

What is abrasion/corrasion?

A

load carried by river rubs against river bed & banks wearing them away

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33
Q

What is solution/corrosion?

A

some rock minerals slowly dissolve in river water, wearing river bed & banks away

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34
Q

What is load?

A

material carried by river

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35
Q

What are the 2 directions of erosion?

A
  • vertical (down) - upper course
  • lateral (sideways) - lower course
36
Q

What is the wetted perimeter?

A

amount of water that comes into contact with the rivers banks & bed

37
Q

How do you calculate wetted perimeter?

A

add up length & width of channel

38
Q

What is traction?

A

large boulders & rocks rolled along river bed

39
Q

What is saltation?

A

small pebbles & stones bounced along river bed

40
Q

What is suspension?

A

fine, light material carried along by river

41
Q

What is solution?

A

minerals dissolved in water, this is a chemical change

42
Q

When does deposition occur?

A

when river doesn’t have enough energy to carry its load, when river slows down & gets shallower

43
Q

Where is deposition most likely to occur?

A

at mouth, inside bend of meander, flood plain

44
Q

What factors affect river discharge?

A
  • temp.
  • vegetation levels
  • urban areas
  • rainfall
  • rock type
  • slope
45
Q

How does temperature affect river discharge?

A

higher temp. causes snow to melt, increasing river discharge

46
Q

How do vegetation levels affect river discharge?

A

high amounts can cause interception, decreasing discharge & increasing lag time

47
Q

How do urban areas affect river discharge?

A

contain impermeable surfaces & can cause an increase in river discharge due to lack of infiltration & increased surface run off, decreasing lag time

48
Q

How does rainfall affect river discharge?

A

high levels can increase discharge, causing a decrease in lag time due to ground being saturated

49
Q

How does rock type affect river discharge?

A

impermeable rock types cause increase in river discharge as water flows over land to river, causing a decrease in lag time

50
Q

How does a slope affect river discharge?

A

steep slopes can increase discharge & decrease lag time as water runs to river faster

51
Q

Which river management strategies are soft management?

A

warning systems
flood plane zoning
afforestation
river restoration
dredging

52
Q

Which river management strategies are hard management?

A

dams
artificial levees & embankments
straightening
flood relief channels

53
Q

What are warning sytems?

A
  • websites, weather apps
  • FEWS - flood early warning systems
  • plan evacuation route
  • add sandbags
    -reduce loss of life
  • homes will still be flooded
54
Q

What are flood plane zones?

A
  • don’t build properties right next to river
  • prevent damage to property
  • some might not be able to access zoning
55
Q

What is afforesation?

A
  • plant trees to increase lag time - interception decreases discharge
  • low cost
  • not that effective
  • long time - trees grow slowly
  • counter deforestation
  • restores natural habitat
56
Q

What is river restoration?

A
  • low cost
  • makes quality worse
  • restores river to its natural state
  • increases erosion
  • expensive initial cost
57
Q

What are dams?

A
  • barrier that stops/restricts flow of water
  • used for irrigation, tourism (boating on reservoir), hydroelectric power
  • expensive
  • disrupts fish habitat/migration
58
Q

What are artificial levees/embankments?

A
  • increase banks of river - reduce discharge
  • prevent lateral erosion
  • expensive
  • ruin look
59
Q

What is straightening?

A
  • removal of meanders - can hold more volume
  • high volume so water can pass through quicker
  • increases risk downstream
60
Q

What is dredging?

A

removal of silt

61
Q

What are flood channels?

A
  • artificial channels to divert water (decreases discharge)
  • pressure of main channels
  • hard to find land
  • expensive
  • if empty can be a place of litter
62
Q

What does the valley cross section of an upper course of a river look like?

A
  • vertical erosion
  • steep sided valley
63
Q

What does the channel cross section of an upper course of a river look like?

A
  • low energy so can’t erode/transport boulders
  • rough channel bed - friction
64
Q

What does the valley cross section of a middle course of a river look like?

A
  • lateral erosion
  • channel occupies far less of total valley
65
Q

What does the channel cross section of a middle course of a river look like?

A
  • smoother channel bed
66
Q

What does the valley cross section of a lower course of a river look like?

A
  • levees/raised banks
  • wide, flat valley
67
Q

What does the channel cross section of a lower course of a river look like?

A
  • very smooth channel: low friction, high velocity
68
Q

How does a river’s cross profile change from source to moutg?

A
  • upper course: valley & channel are narrow & deep due to large amount of vertical erosion
  • sides of river’s valley are steep (v-shaped valley)
  • channel occupies majority of valley floor
  • more downstream: valley increases in width
  • channel depth doesn’t change much as vertical erosion as slowed
  • sides of valley become more gentle
  • rivers channel occupies little of valley floor
69
Q

What opportunities are associated with rivers

A
  • agriculture - fertile silt & soil, so areas are intensively farmed, repeated flooding replenishes nutrients taken by plants, provides water for irrigating crops
  • trade - many successful cities built by rivers to provide trade routes to other countries & continents
  • leisure - boating, rowing swimming…
  • energy - source of power for mills & factory machinery, modern tech allows electricity production from large dams e.g. 3 Gorges dam (China)
  • homes - floodplains provide flat building land, river water can be used for drinking, washing & cooking
70
Q

What do long profiles show?

A

how a rivers gradient changes

71
Q

What do cross profiles show?

A

a cross-section of a channel & valley at certain points in rivers course

72
Q

What would a long & cross profile show of the upper course of a river?

A
  • steep gradient
  • low total load
  • slow average velocity
  • vertical erosion
  • big particle size
  • rapids/waterfalls
73
Q

What would a long & cross profile show of the middle course of a river?

A
  • less steep
  • increasing total load
  • increasing average velocity
  • increasing discharge/volume
  • decreasing particle size
  • meanders/oxbow lakes
  • lateral erosion
74
Q

What would a long & cross profile show of the lower course of a river?

A
  • flattest gradient
  • highest total load
  • smallest particle size
  • fastest average velocity (until mouth)
  • flood planes & deltas
75
Q

Why do we care about flooding?

A
  • can cause damage to homes/businesses, infrastructure & communications
  • social problems - homelessness/injury/death
  • economic problems - cost of repair/loss of businesses
  • environmental problems - damage to crops/destroying animal habitats
76
Q

What are hard engineering strategies?

A

building artificial structures that try to control rivers

77
Q

What are soft engineering strategies?

A

doesn’t involve building artificial structures, but takes a more sustainable & natural approach to managing potential for flooding

78
Q

What is lag time?

A

shorter the lag time, flashier the flood

79
Q

What is alluvium?

A

fine, fertile sediment depostied on a flood plane

80
Q

What is the Mekong Delta used for?

A
  • domestic use (cooking & cleaning)
  • transport
  • irrigation (moving water to fields to water crops)
  • trade & tourism (floating market)
81
Q

Statistics about the Mekong Delta

A
  • one of the most intently farmed areas in Asia
  • Vietnam is 2nd biggest rice exports in the world
  • 80% who live there are farmers
  • catching 50kg fish per day = $70,000 per year
  • GDP per capita >$4,000
  • 90% Vietnam’s population live in countryside using waters of the Mekong
  • 11 dams in lower course of Mekong provides electricity for millions in Vietnam & Laos
82
Q

Where are the Somerset Levels?

A

coastal plains & wetlands in Somerset, SW England

83
Q

What rivers flow through the Somerset Levels?

A

River Tone & Parrett, drain into Bristol channel

84
Q

What were the physical causes of the Somerset Floods?

A
  • rain - low pressure caused heavy rain off the Atlantic, causing 350mm rain In Jan & Feb (10mm above average)
  • high tides - storm surges caused high tides, preventing freshwater from draining into sea
  • dredging - hadn’t been dredged in over 20 years
85
Q

What were the human causes of the Somerset Floods?

A
  • much land been converted from grassland to grow maise
  • ground able to retain less water
  • causing surface runoff
86
Q

What were the social impacts of the Somerset Floods?

A
  • over 600 homes flooded
  • 16 farms evacuated
  • power supplies cut off
  • villages (e.g. Moorland) cut off completely & people left stranded
87
Q

What were the social impacts of the Somerset Floods?

A
  • cost damage estimated over £10m
  • over 140km² agricultural land underwater for 3-4 weeks
  • 1000 livestock evacuated
  • Bristol to Taunton railways line closed
88
Q

What were the environmental impacts of the Somerset Floods?

A
  • sewage, chemicals (e.g. pesticides) contaminated floodwater & it spread to other areas
  • destroyed ecosystems & limited food supply for animals
89
Q

What were the immediate responses of the Somerset Floods?

A
  • warning (amber alert from MetOffice)
  • placed sandbags in front of buildings
  • man in Moorland made large wall out of clay & mud to protect his house from flooding
  • 80 homes evacuated
  • fire brigade rescued people on boats
  • 65 pumps used to drain 65mil m³ floodwater
  • government provided £15m
90
Q

What were the long-term responses of the Somerset Floods?

A
  • Somerset Levels & Moors Action Plan reintroduced dredging, constructing a tidal barrage & additional permanent pumping stations
  • part of a 20 year plan for Somerset Levels that will total £100m